This report contains detailed petrographic descriptions of 74 thin sections from drill hole USW G-1 at Yucca Mountain, Nevada. These descriptions are keyed to the distinctions between devitrified, vitrophyre, vitric, and zeolitized intervals below the Topopah Spring Member repository horizon. The petrographic features of the zeolitized intervals down through the Crater Flat tuff, as well as the sorption properties determined from these intervals, suggest that these zeolite occurrences may each have comparable sorptive capability
Yucca Mountain, a > 1.5-km thick sequence of tuffs and subordinate lavas in southwest Nevada, is bei...
Fracture-lining minerals are being studied as part of site characterization to determine the suitabi...
Yucca Mountain, a >1.5-km-thick sequence of tuffs and subordinate lavas in southwest Nevada, is bein...
The Topopah Spring Member of the Paintbrush Tuff and the Lithic-rich tuff and two Tertiary volcanic ...
Quantitative X-ray powder diffraction methods have been used to analyze 108 samples from drill core ...
Tuffs of the Nevada Test Site are currently under investigation to determine their potential for lon...
Quantitative x-ray powder diffraction analysis of tuffs and silicic lavas, using matrix-flushing tec...
This report is a compilation of petrographic and mineral chemical data for stratigraphic units at Yu...
Lithostratigraphic relations within the Calico Hills Formation and Prow Pass Tuff (Crater Flat Group...
Drill hole UE25a-1 has penetrated tuffs of Tertiary age which contain two major zeolitized horizons ...
This study describes and interprets petrochemical variation of the matrix (excluding fractures and l...
This paper describes the distribution and chemistry of zeolites in tuffs and in fractures at Yucca M...
Petrologic, bulk chemical and mineralogic data are presented for 19 samples of tuffaceous rocks from...
Yucca Mountain in southwestern Nevada is a prominent, irregularly shaped upland formed by a thick ap...
The Yucca Mountain Site Characterization Project is investigating Yucca Mountain, Nevada, as a poten...
Yucca Mountain, a > 1.5-km thick sequence of tuffs and subordinate lavas in southwest Nevada, is bei...
Fracture-lining minerals are being studied as part of site characterization to determine the suitabi...
Yucca Mountain, a >1.5-km-thick sequence of tuffs and subordinate lavas in southwest Nevada, is bein...
The Topopah Spring Member of the Paintbrush Tuff and the Lithic-rich tuff and two Tertiary volcanic ...
Quantitative X-ray powder diffraction methods have been used to analyze 108 samples from drill core ...
Tuffs of the Nevada Test Site are currently under investigation to determine their potential for lon...
Quantitative x-ray powder diffraction analysis of tuffs and silicic lavas, using matrix-flushing tec...
This report is a compilation of petrographic and mineral chemical data for stratigraphic units at Yu...
Lithostratigraphic relations within the Calico Hills Formation and Prow Pass Tuff (Crater Flat Group...
Drill hole UE25a-1 has penetrated tuffs of Tertiary age which contain two major zeolitized horizons ...
This study describes and interprets petrochemical variation of the matrix (excluding fractures and l...
This paper describes the distribution and chemistry of zeolites in tuffs and in fractures at Yucca M...
Petrologic, bulk chemical and mineralogic data are presented for 19 samples of tuffaceous rocks from...
Yucca Mountain in southwestern Nevada is a prominent, irregularly shaped upland formed by a thick ap...
The Yucca Mountain Site Characterization Project is investigating Yucca Mountain, Nevada, as a poten...
Yucca Mountain, a > 1.5-km thick sequence of tuffs and subordinate lavas in southwest Nevada, is bei...
Fracture-lining minerals are being studied as part of site characterization to determine the suitabi...
Yucca Mountain, a >1.5-km-thick sequence of tuffs and subordinate lavas in southwest Nevada, is bein...